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Volume 17 Issue 4
Dec 2006
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Nengsong CHEN, Songlin GONG, Min SUN, Yong YANG, Rong LIU. How High Are the P-T Conditions for Paleoproterozoic Metamorphism of the Huangtuling Felsic Granulite, North Dabieshan, Central China?. Journal of Earth Science, 2006, 17(4): 291-301.
Citation: Nengsong CHEN, Songlin GONG, Min SUN, Yong YANG, Rong LIU. How High Are the P-T Conditions for Paleoproterozoic Metamorphism of the Huangtuling Felsic Granulite, North Dabieshan, Central China?. Journal of Earth Science, 2006, 17(4): 291-301.

How High Are the P-T Conditions for Paleoproterozoic Metamorphism of the Huangtuling Felsic Granulite, North Dabieshan, Central China?

Funds:

Special Doctoral Grant of the Ministry ofEducation of China 98049114

National Natural Science Foundation of China 49972023

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  • Corresponding author: Chen Nengsong: nengsongchen@cug.edu.cn
  • Received Date: 09 Jul 2006
  • Accepted Date: 25 Sep 2006
  • The 2.34 cm-wide garnet porphyroblast in the Paleoproterozoic felsic granulite from the Huangtuling area, North Dabieshan, has been reinvestigated for compositional variation in light of Ca-composition X-ray mapping to obtain peak P-T conditions of granulite-facies metamorphism. A new core-rim traverse was conducted through where there is little influence on Ca-profile and slight modification in Mn-, Mg- and Fe-profiles with the highest Mg/ (Mg+Fe) value of 0.467. Reasonable peak P-T conditions were estimated to be 1.50-1.70 GPa and 1 100-1 150 ℃ according to TWQ-based garnet-Al-orthopyroxene thermobarometry. These estimations suggest that the Huangtuling granulite once was subjected to ultrahigh-temperature (UHT) granulite-facies metamorphism following a high-pressure granulite-faices metamorphic stage, implying that a deep subduction and collision process relevant to the Yangtze block occurred in the Paleoproterozoic time, probably as a response to the global assembly event of the Columbia supercontinent.

     

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